Abstract
Following the fragment asperity interaction model introduced by
Sotolongo-Costa and Posadas (2004) and revised by Silva et al. (2006),
we try to explain the nonextensive effect in the context of the asperity
model designed by Lay and Kanamori (1981). To address this issue, we
used data from the NEIC catalog in the decade between 2001 and 2010, in
order to investigate the so-called Circum-Pacific subduction zones. We
propose a geophysical explanation to nonextensive parameter q. The
results need further investigation however evidence of correlation
between the nonextensive parameter and the asperity model is shown,
i.e., we show that q-value is higher for areas with larger asperities
and stronger coupling. (C) 2015 Elsevier B.V. All rights reserved.
Users
Please
log in to take part in the discussion (add own reviews or comments).